Palynostratigraphy of the South African Karoo supergroup and correlations with coeval Gondwanan successions

Autor: Barbolini, Natasha

The Main Karoo Basin of South Africa is renowned for its exceptional palaeontological record and while its vertebrate fossils have been extensively researched, Karoo floras have received considerably less attention. Poor yields of palynomorphs from t

Externí odkaz: http://hdl.handle.net10539/14776

Palynology of a coal seam in Karoo deposits of Botswana and correlation with southern African coal-bearing strata

Autor: Barbolini, Natasha

A significant amount of palynological work has been done on southern African coal seams in the Ecca Group, but as yet there is little consensus on how these areas relate to each other. This study investigated the palynology of a coal seam from Mmaman

Externí odkaz: http://hdl.handle.net/10539/8904

Resolving the age of Madumabisa fossil vertebrates: Palynological evidence from the mid-Zambezi Basin of Zambia

Autor: Barbolini, Natasha, Smith, Roger M.H., Tabor, Neil J., Sidor, Christian A., Angielczyk, Kenneth D.

Publikováno v: In Palaeogeography, Palaeoclimatology, Palaeoecology 1 September 2016 457:117-128

Marine flooding surfaces recorded in Permian black shales and coal deposits of the Main Karoo Basin (South Africa): Implications for basin dynamics and cross-basin correlation: Discussion

Autor: Cole, Doug, Barbolini, Natasha

Publikováno v: In International Journal of Coal Geology 15 May 2019 209:130-131

Quelle influence du forçage orbital sur le climat et les biomesde l'Éocène et de l'Oligocène ?

Autor: Tardif, Delphine, Toumoulin, Agathe, Fluteau, Frédéric, Donnadieu, Yannick, Le Hir, Guillaume, Licht, Alexis, Dupont-Nivet, Guillaume, Barbolini, Natasha, Hoorn, Carina, Ladant, Jean Baptiste, Sepulchre, Pierre, Viovy, Nicolas

Publikováno v: 27 ème Réunion des sciences de la Terre (RST 2021)
27 ème Réunion des sciences de la Terre (RST 2021), SGF, CNRS, Laboratoire de Géologie de Lyon ou l’étude de la Terre, des planètes et de l’environnement, Nov 2021, Lyon, France. pp.611

National audience; La transition de l'Éocène Greenhouse vers l'Oligocène Icehouse (∼40 à 32 Ma)résulte de l'interaction entre une baisse du CO2, des changements paléogéographiqueset le forçage orbital. Cependant, son expression en termes de

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::a045d4c41a4934089ace7a2b1bc6e2fa
https://insu.hal.science/insu-03522556